Mining lakes as groundwater‐dominated hydrological systems: assessment of the water balance of Mining Lake Plessa 117 (Lusatia, Germany) using stable isotopes

Medientyp: E-Artikel
Titel: Mining lakes as groundwater‐dominated hydrological systems: assessment of the water balance of Mining Lake Plessa 117 (Lusatia, Germany) using stable isotopes
Beteiligte: Hofmann, Hilmar; Knöller, Kay; Lessmann, Dieter
Erschienen: Wiley, 2008
Erschienen in: Hydrological Processes
Sprache: Englisch
DOI: 10.1002/hyp.7071
ISSN: 0885-6087; 1099-1085
Schlagwörter: Water Science and Technology
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Beschreibung: <jats:title>Abstract</jats:title><jats:p>In the present study, the stable isotopes δ<jats:sup>18</jats:sup>O and δ<jats:sup>2</jats:sup>H were used for assessment of the water balance in a heterogeneously structured catchment area in the Lusatian Lignite Mining District, in particular, for estimation of the annual groundwater inflow and outflow (<jats:italic>I</jats:italic><jats:sub><jats:italic>GW</jats:italic></jats:sub> and <jats:italic>O</jats:italic><jats:sub><jats:italic>GW</jats:italic></jats:sub>) of Mining Lake Plessa 117. The application of stable isotopes was possible since the water exchange in the catchment area had reached steady‐state conditions after the abandonment of mining activities in 1968 and the filling of the voids and aquifers by re‐rising groundwater in the years thereafter. Diverging slopes of the Evaporation Line and the Global Meteoric Water Line manifested as evaporation from the lake catchment area. The calculated isotope water balance was compared with the commonly used surface water balance, which is unable to differentiate between <jats:italic>I</jats:italic><jats:sub><jats:italic>GW</jats:italic></jats:sub> and <jats:italic>O</jats:italic><jats:sub><jats:italic>GW</jats:italic></jats:sub>, and with a local groundwater model. The groundwater model calculated an <jats:italic>I</jats:italic><jats:sub><jats:italic>GW</jats:italic></jats:sub> of about 811 000 m<jats:sup>3</jats:sup> yr<jats:sup>−1</jats:sup> and an <jats:italic>O</jats:italic><jats:sub><jats:italic>GW</jats:italic></jats:sub> close to zero, whereas the isotope water balance showed fluxes of about 914 000 and 140 000 m<jats:sup>3</jats:sup> yr<jats:sup>−1</jats:sup>, respectively. Considering the contribution of the groundwater inflow to the total annual input into the lake (Δ<jats:italic>I</jats:italic><jats:sub><jats:italic>T</jats:italic></jats:sub>) and the mean residence time (τ), where the groundwater model and the isotope water balance calculated 42 and 47% for Δ<jats:italic>I</jats:italic><jats:sub><jats:italic>T</jats:italic></jats:sub> and 4·3 and 3·9 years for τ, respectively, it was shown that both water balance calculation methods led to comparable results despite the differences in <jats:italic>I</jats:italic><jats:sub><jats:italic>GW</jats:italic></jats:sub> and <jats:italic>O</jats:italic><jats:sub><jats:italic>GW</jats:italic></jats:sub>. Copyright © 2008 John Wiley & Sons, Ltd.</jats:p>

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